van Drecht G, Bouwman A F, Knoop J M, Meinardi C, Beusen A
National Institute of Public Health and the Environmrnt, Bilthoven, The Netherlands.
ScientificWorldJournal. 2001 Nov 6;1 Suppl 2:632-41. doi: 10.1100/tsw.2001.326.
Global 0.5- by 0.5-degree resolution estimates are presented on the fate of nitrogen (N) stemming from point and nonpoint sources, including plant uptake, denitrification, leaching from the rooting zone, rapid flow through shallow groundwater, and slow flow through deep groundwater to riverine systems. Historical N inputs are used to describe the N flows in groundwater. For nonpoint N sources (agricultural and natural ecosystems), calculations are based on local hydrology, climate, geology, soils, climate and land use combined with data for 1995 on crop production, N inputs from N fertilizers and animal manure, and estimates for ammonia emissions, biological N fixation, and N deposition. For point sources, our estimates are based on population densities and human N emissions, sanitation, and treatment. The results provide a first insight into the magnitude of the N losses from soil-plant systems and point sources in various parts of the world, and the fate of N during transport in atmosphere, groundwater, and surface water. The contribution to the river N load by anthropogenic N pollution is dominant in many river basins in Europe, Asia, and North Africa. Our model results explain much of the variation in measured N export from different world river basins.
给出了全球0.5×0.5度分辨率下关于点源和非点源氮(N)归宿的估计,包括植物吸收、反硝化作用、根区淋溶、浅层地下水快速流动以及深层地下水缓慢流入河流系统。利用历史氮输入量来描述地下水中的氮流动情况。对于非点源氮(农业和自然生态系统),计算基于当地水文、气候、地质、土壤、气候和土地利用情况,并结合1995年的作物产量数据、氮肥和动物粪便的氮输入量以及氨排放、生物固氮和氮沉降的估计值。对于点源,我们的估计基于人口密度、人类氮排放、卫生设施和处理情况。这些结果首次揭示了世界不同地区土壤-植物系统和点源氮损失的规模,以及氮在大气、地下水和地表水传输过程中的归宿。在欧洲、亚洲和北非的许多流域,人为氮污染对河流氮负荷的贡献占主导地位。我们的模型结果解释了不同世界流域实测氮输出变化的很大一部分原因。